An Analysis of Genesis and Ore Control Factor of Huangcaoling Pb-Zn Deposit in Zhenyuan, Yunnan
详细信息   
摘要

///The orefield is in the S end part of Lanping-Puer Mesozoic foreland basin. The ore-bearing bed is the pale-color fine clastic rock with intercalation of Ca-Mn layer of upper part of Jingxing Formation Lower Member. The ore deposit is controlled strictly by the fault and fracture zone. It is a typical mid-low T Pb-Zn deposit of sedimentation reformation.
    
    

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